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  • 1. Aggarwal, Pradeep K.
    et al.
    Romatschke, Ulrike
    Araguas-Araguas, Luis
    Belachew, Dagnachew
    Longstaffe, Frederick J.
    Berg, Peter
    SMHI, Research Department, Hydrology.
    Schumacher, Courtney
    Funk, Aaron
    Proportions of convective and stratiform precipitation revealed in water isotope ratios2016In: Nature Geoscience, ISSN 1752-0894, E-ISSN 1752-0908, Vol. 9, no 8, p. 624-+Article in journal (Refereed)
  • 2.
    Berg, Peter
    et al.
    SMHI, Research Department, Climate research - Rossby Centre.
    Moseley, Christopher
    Haerter, Jan O.
    Strong increase in convective precipitation in response to higher temperatures2013In: Nature Geoscience, ISSN 1752-0894, E-ISSN 1752-0908, Vol. 6, no 3, p. 181-185Article in journal (Refereed)
    Abstract [en]

    Precipitation changes can affect society more directly than variations in most other meteorological observables(1-3), but precipitation is difficult to characterize because of fluctuations on nearly all temporal and spatial scales. In addition, the intensity of extreme precipitation rises markedly at higher temperature(4-9), faster than the rate of increase in the atmosphere's water-holding capacity(1,4), termed the Clausius-Clapeyron rate. Invigoration of convective precipitation (such as thunderstorms) has been favoured over a rise in strati-form precipitation (such as large-scale frontal precipitation) as a cause for this increase(4,10), but the relative contributions of these two types of precipitation have been difficult to disentangle. Here we combine large data sets from radar measurements and rain gauges over Germany with corresponding synoptic observations and temperature records, and separate convective and stratiform precipitation events by cloud observations. We find that for stratiform precipitation, extremes increase with temperature at approximately the Clausius-Clapeyron rate, without characteristic scales. In contrast, convective precipitation exhibits characteristic spatial and temporal scales, and its intensity in response to warming exceeds the Clausius-Clapeyron rate. We conclude that convective precipitation responds much more sensitively to temperature increases than stratiform precipitation, and increasingly dominates events of extreme precipitation.

  • 3. Bertola, Miriam
    et al.
    Bloeschl, Guenter
    Bohac, Milon
    Borga, Marco
    Castellarin, Attilio
    Chirico, Giovanni B.
    Claps, Pierluigi
    Dallan, Eleonora
    Danilovich, Irina
    Ganora, Daniele
    Gorbachova, Liudmyla
    Ledvinka, Ondrej
    Mavrova-Guirguinova, Maria
    Montanari, Alberto
    Ovcharuk, Valeriya
    Viglione, Alberto
    Volpi, Elena
    Arheimer, Berit
    SMHI, Research Department, Hydrology.
    Aronica, Giuseppe Tito
    Bonacci, Ognjen
    Canjevac, Ivan
    Csik, Andras
    Frolova, Natalia
    Gnandt, Boglarka
    Gribovszki, Zoltan
    Guel, Ali
    Guenther, Knut
    Guse, Bjoern
    Hannaford, Jamie
    Harrigan, Shaun
    Kireeva, Maria
    Kohnova, Silvia
    Komma, Juergen
    Kriauciuniene, Jurate
    Kronvang, Brian
    Lawrence, Deborah
    Luedtke, Stefan
    Mediero, Luis
    Merz, Bruno
    Molnar, Peter
    Murphy, Conor
    Oskorus, Dijana
    Osuch, Marzena
    Parajka, Juraj
    Pfister, Laurent
    Radevski, Ivan
    Sauquet, Eric
    Schroeter, Kai
    Sraj, Mojca
    Szolgay, Jan
    Turner, Stephen
    Valent, Peter
    Veijalainen, Noora
    Ward, Philip J.
    Willems, Patrick
    Zivkovic, Nenad
    Megafloods in Europe can be anticipated from observations in hydrologically similar catchments2023In: Nature Geoscience, ISSN 1752-0894, E-ISSN 1752-0908Article in journal (Refereed)
    Download full text (pdf)
    Megafloods in Europe can be anticipated from observations in hydrologically similar catchments
  • 4. Moseley, Christopher
    et al.
    Hohenegger, Cathy
    Berg, Peter
    SMHI, Research Department, Hydrology.
    Haerter, Jan O.
    Intensification of convective extremes driven by cloud-cloud interaction2016In: Nature Geoscience, ISSN 1752-0894, E-ISSN 1752-0908, Vol. 9, no 10, p. 748-+Article in journal (Refereed)
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